Zobrazeno 1 - 4
of 4
pro vyhledávání: '"A. M. E. Winguth"'
Autor:
D. J. Lunt, M. Huber, E. Anagnostou, M. L. J. Baatsen, R. Caballero, R. DeConto, H. A. Dijkstra, Y. Donnadieu, D. Evans, R. Feng, G. L. Foster, E. Gasson, A. S. von der Heydt, C. J. Hollis, G. N. Inglis, S. M. Jones, J. Kiehl, S. Kirtland Turner, R. L. Korty, R. Kozdon, S. Krishnan, J.-B. Ladant, P. Langebroek, C. H. Lear, A. N. LeGrande, K. Littler, P. Markwick, B. Otto-Bliesner, P. Pearson, C. J. Poulsen, U. Salzmann, C. Shields, K. Snell, M. Stärz, J. Super, C. Tabor, J. E. Tierney, G. J. L. Tourte, A. Tripati, G. R. Upchurch, B. S. Wade, S. L. Wing, A. M. E. Winguth, N. M. Wright, J. C. Zachos, R. E. Zeebe
Publikováno v:
Geoscientific Model Development, Vol 10, Iss 2, Pp 889-901 (2017)
Past warm periods provide an opportunity to evaluate climate models under extreme forcing scenarios, in particular high ( > 800 ppmv) atmospheric CO2 concentrations. Although a post hoc intercomparison of Eocene ( ∼ 50 Ma) climate model simulations
Externí odkaz:
https://doaj.org/article/f7eaea5171304bb78e8d55e7d251702b
Publikováno v:
Biogeosciences, Vol 14, Iss 4, Pp 781-797 (2017)
Dissolved oxygen (DO) concentration in the ocean is an important component of marine biogeochemical cycles and will be greatly altered as climate change persists. In this study a global oceanic carbon cycle model (HAMOCC 2.0) is used to address how m
Externí odkaz:
https://doaj.org/article/f4473ca1220248f9946531139117c8f7
Autor:
A. M. E. Winguth, J. F. Tjiputra
Publikováno v:
Biogeosciences, Vol 5, Iss 2, Pp 615-630 (2008)
An adjoint model is applied to examine the biophysical factors that control surface pCO2 in different ocean regions. In the tropical Atlantic and Indian Oceans, the annual cycle of pCO2 in the model is highly dominated by temperature variability, whe
Externí odkaz:
https://doaj.org/article/d9c2bd25c18b4c0997e533e9ff7c007c
